Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal
Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average a...
Published in: | Journal of Glaciology |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1978
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000033931 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033931 |
_version_ | 1821563375389245440 |
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author | Haida, Osamu Suga, Hiroshi Seki, Syūzō |
author_facet | Haida, Osamu Suga, Hiroshi Seki, Syūzō |
author_sort | Haida, Osamu |
collection | Cambridge University Press |
container_issue | 85 |
container_start_page | 707 |
container_title | Journal of Glaciology |
container_volume | 21 |
description | Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average activation enthalpy of the relaxational process was determined to be (26±5) kJ mol -1 . Residual entropies of the crystal were recalculated on the basis of the present heat-capacity data combined with the revised values for enthalpy of vaporization, saturated vapour pressure, and spectroscopic entropy. They are (3.47±0.41 J K -1 mol -1 for the quenched crystal and (3.44±0.41) J K -1 mol -1 for a crystal annealed at 102-106 K for 264 h. The characteristics and the origin of the anomaly are discussed in comparison with that of ordinary ice. This paper has been accepted for publication in full in a forthcoming issue of the Journal of Glaciology . |
format | Article in Journal/Newspaper |
genre | Journal of Glaciology |
genre_facet | Journal of Glaciology |
id | crcambridgeupr:10.1017/s0022143000033931 |
institution | Open Polar |
language | English |
op_collection_id | crcambridgeupr |
op_doi | https://doi.org/10.1017/s0022143000033931 |
op_source | Journal of Glaciology volume 21, issue 85, page 707 ISSN 0022-1430 1727-5652 |
publishDate | 1978 |
publisher | Cambridge University Press (CUP) |
record_format | openpolar |
spelling | crcambridgeupr:10.1017/s0022143000033931 2025-01-16T22:46:33+00:00 Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal Haida, Osamu Suga, Hiroshi Seki, Syūzō 1978 http://dx.doi.org/10.1017/s0022143000033931 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033931 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 707 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033931 2024-02-08T08:36:10Z Abstract The heat capacities of quenched and annealed heavy ice Ih were measured in the temperature range 14 to 300 K by an adiabatic calorimeter. A relaxational thermal anomaly was found at around 115 K and this phenomenon was ascribed to the onset of deuteron ordering in the crystal. The average activation enthalpy of the relaxational process was determined to be (26±5) kJ mol -1 . Residual entropies of the crystal were recalculated on the basis of the present heat-capacity data combined with the revised values for enthalpy of vaporization, saturated vapour pressure, and spectroscopic entropy. They are (3.47±0.41 J K -1 mol -1 for the quenched crystal and (3.44±0.41) J K -1 mol -1 for a crystal annealed at 102-106 K for 264 h. The characteristics and the origin of the anomaly are discussed in comparison with that of ordinary ice. This paper has been accepted for publication in full in a forthcoming issue of the Journal of Glaciology . Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 707 |
spellingShingle | Earth-Surface Processes Haida, Osamu Suga, Hiroshi Seki, Syūzō Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title | Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_full | Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_fullStr | Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_full_unstemmed | Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_short | Enthalpy Relaxation Phenomenon in a Heavy Ice Crystal |
title_sort | enthalpy relaxation phenomenon in a heavy ice crystal |
topic | Earth-Surface Processes |
topic_facet | Earth-Surface Processes |
url | http://dx.doi.org/10.1017/s0022143000033931 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033931 |